A type of detachment fault system that is
characterized by different styles of deformation above and
below the fault plane. They are typically associated with
large-scale thrusting and folding of the thrust sheet overlying
the fault, with the rocks underneath the fault remaining relatively
undeformed. Decollement faults originate as relatively
flat lying but may become rotated to steeper attitudes in progressive
or younger deformation events. Beautifully exposed
decollement faults are known from the American and Canadian
Rockies, the Alps, and many other mountain belts
around the world.
See also STRUCTURAL GEOLOGY.














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